Volume 123, Issue 44 pp. 10524-10527
Zuschrift

Molecular Storage of Ozone in a Clathrate Hydrate Formed from an O3+O2+CO2 Gas Mixture

Takahiro Nakajima

Takahiro Nakajima

Department of Mechanical Engineering, Keio University, 3-14-1 Hiyoshi, Kohoku-ku, Yokohama 223-8522 (Japan)

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Satoru Akatsu

Satoru Akatsu

Department of Mechanical Engineering, Keio University, 3-14-1 Hiyoshi, Kohoku-ku, Yokohama 223-8522 (Japan)

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Dr. Ryo Ohmura

Dr. Ryo Ohmura

Department of Mechanical Engineering, Keio University, 3-14-1 Hiyoshi, Kohoku-ku, Yokohama 223-8522 (Japan)

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Dr. Satoshi Takeya

Dr. Satoshi Takeya

Research Institute of Instrumentation Frontier, National Institute of Advanced Industrial Science and Technology (AIST), Central 5, Higashi 1-1-1, Tsukuba 305-8565 (Japan)

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Dr. Yasuhiko H. Mori

Corresponding Author

Dr. Yasuhiko H. Mori

Department of Mechanical Engineering, Keio University, 3-14-1 Hiyoshi, Kohoku-ku, Yokohama 223-8522 (Japan)

Department of Mechanical Engineering, Keio University, 3-14-1 Hiyoshi, Kohoku-ku, Yokohama 223-8522 (Japan)Search for more papers by this author
First published: 14 September 2011
Citations: 8

This study was supported in part by a Grant-in-Aid for the Global COE Program for the “Center for Education and Research of Symbiotic, Safe and Secure System Design” from the Ministry of Education, Culture, Sport and Technology (Japan). The authors thank Fumihito Takeuchi, a former student in Keio University, for his help in the preliminary stages of this study.

Graphical Abstract

Ozon auf Eis gelegt: Aus einer O3+O2+CO2-Gasmischung kann ein Clathrat-Hydrat gebildet werden (links im Bild; das O2+CO2-Hydrat ist zum Vergleich gezeigt), dessen blassblaue Farbe wahrscheinlich von den darin eingeschlossenen Ozonmolekülen herrührt. An Luft bei Normaldruck und −25 °C bleibt das Ozon (0.1 % Massenanteil) im O3+O2+CO2-Hydrat mehr als vier Wochen lang erhalten.

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